Soil Data Explorer - CORRALITOS

Official Series Description

Lab Data Summary

Aggregate lab data for the CORRALITOS soil series. This aggregation is based on all pedons with a current taxon name of CORRALITOS, and applied along 1-cm thick depth slices. Solid lines are the slice-wise median, bounded on either side by the interval defined by the slice-wise 5th and 95th percentiles. The median is the value that splits the data in half. Five percent of the data are less than the 5th percentile, and five percent of the data are greater than the 95th percentile. Values along the right hand side y-axis describe the proportion of pedon data that contribute to aggregate values at this depth. For example, a value of "90%" at 25cm means that 90% of the pedons correlated to CORRALITOS were used in the calculation. Source: KSSL snapshot (updated 2020-03-13). Methods used to assemble the KSSL snapshot used by SoilWeb / SDE

There are insufficient data to create the lab data summary figure.

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the CORRALITOS soil series. Monthly precipitation (PPT) and potential evapotranspiration (PET) have been estimated from the 50th percentile of gridded values (PRISM 1981-2010) overlapping with the extent of SSURGO map units containing each series as a major component. Monthly PET values were estimated using the method of Thornthwaite (1948). These (and other) climatic parameters are calculated with each SSURGO refresh and provided by the fetchOSD function of the soilDB package. Representative water storage values (“AWC” in the figures) were derived from SSURGO by taking the 50th percentile of profile-total water storage (sum[awc_r * horizon thickness]) for each soil series. Note that this representation of “water storage” is based on the average ability of most plants to extract soil water between 15 bar (“permanent wilting point”) and 1/3 bar (“field capacity”) matric potential. Soil moisture state can be roughly interpreted as “dry” when storage is depleted, “moist” when storage is between 0mm and AWC, and “wet” when there is a surplus. Clearly there are a lot of assumptions baked into this kind of monthly water balance. This is still a work in progress.

Sibling Summary

Siblings are those soil series that occur together in map units, in this case with the CORRALITOS series. Sketches are arranged according to their subgroup-level taxonomic structure. Source: SSURGO snapshot (updated 2024-10-24), parsed OSD records (updated 2024-10-23) and snapshot of SC database (updated 2024-10-23).

Select annual climate data summaries for the CORRALITOS series and siblings. Series are sorted according to hierarchical clustering of median values. Source: SSURGO map unit geometry and 1981-2010, 800m PRISM data (updated 2024-10-23).

Geomorphic description summaries for the CORRALITOS series and siblings. Series are sorted according to hierarchical clustering of proportions and relative hydrologic position within an idealized landform (e.g. top to bottom). Most soil series (SSURGO components) are associated with a hillslope position and one or more landform-specific positions: hills, mountain slopes, terraces, and/or flats. Proportions can be interpreted as an aggregate representation of geomorphic membership. The values printed to the left (number of component records) and right (Shannon entropy) of stacked bars can be used to judge the reliability of trends. Small Shannon entropy values suggest relatively consistent geomorphic association, while larger values suggest lack thereof. Source: SSURGO component records (updated 2024-10-23).

Competing Series

Soil series competing with CORRALITOS share the same family level classification in Soil Taxonomy. Source: parsed OSD records (updated 2024-10-23) and snapshot of the SC database (updated 2024-10-23).

Select annual climate data summaries for the CORRALITOS series and competing. Series are sorted according to hierarchical clustering of median values. Source: SSURGO map unit geometry and 1981-2010, 800m PRISM data (updated 2024-10-23).

Geomorphic description summaries for the CORRALITOS series and competing. Series are sorted according to hierarchical clustering of proportions and relative hydrologic position within an idealized landform (e.g. top to bottom). Proportions can be interpreted as an aggregate representation of geomorphic membership. Most soil series (SSURGO components) are associated with a hillslope position and one or more landform-specific positions: hills, mountain slopes, terraces, and/or flats. The values printed to the left (number of component records) and right (Shannon entropy) of stacked bars can be used to judge the reliability of trends. Shannon entropy values close to 0 represent soil series with relatively consistent geomorphic association, while values close to 1 suggest lack thereof. Source: SSURGO component records (updated 2024-10-23).

Soil series sharing subgroup-level classification with CORRALITOS, arranged according to family differentiae. Hovering over a series name will print full classification and a small sketch from the OSD. Source: snapshot of SC database (updated 2024-10-23).

Block Diagrams

No block diagrams are available.

Map Units

Map units containing CORRALITOS as a major component. Limited to 250 records.

Map Unit Name	Symbol	Map Unit Area (ac)	Map Unit Key	National Map Unit Symbol	Soil Survey Area	Publication Date	Map Scale
Corralitos loamy sand, 2 to 9 percent slopes	CuC	375	693537	r8p5	ca053	1972	1:24000
Corralitos loamy sand, 2 to 9 percent slopes	CuC	365	456177	h9pd	ca069	1965	1:20000
Corralitos sandy loam, nearly level, imperfectly draine d	CtA	200	456358	h9w7	ca637	1958	1:15000
Corralitos sandy loam, gently sloping	CsB	172	456357	h9w6	ca637	1958	1:15000
Corralitos sandy loam, over clay, nearly level, imperfe ctly drained	CyA	151	456362	h9wc	ca637	1958	1:15000
Corralitos sandy loam, over gravel, nearly level, imper fectly drained	CuA	109	456360	h9w9	ca637	1958	1:15000
Corralitos sandy loam, nearly level	CsA	66	456356	h9w5	ca637	1958	1:15000
Corralitos loamy sand, nearly level, imperfectly draine d	CrA	59	456355	h9w4	ca637	1958	1:15000
Corralitos sandy loam, gently sloping, imperfectly drai ned	CtB	42	456359	h9w8	ca637	1958	1:15000
Corralitos sandy loam, over gravel, gently sloping	CwB	19	456361	h9wb	ca637	1958	1:15000
Corralitos loamy sand, 5 to 9 percent slopes	CsC	2862	456786	hbb1	ca638	1967	1:24000
Corralitos loamy sand, 9 to 15 percent slopes	CsD	2000	456787	hbb2	ca638	1967	1:24000
Corralitos loamy sand, 0 to 5 percent slopes	CsB	1650	456785	hbb0	ca638	1967	1:24000
Corralitos sand, 2 to 15 percent slopes	125	1310	457097	hbn2	ca664	1977	1:24000
Corralitos sand, 0 to 2 percent slopes	124	695	457096	hbn1	ca664	1977	1:24000
Corralitos variant loamy sand	126	385	457098	hbn3	ca664	1977	1:24000
Corralitos loamy sand, 0 to 2 percent slopes	CuA	4004	457376	hby2	ca672	1966	1:20000
Corralitos sand, 2 to 15 percent slopes	CtD	3569	457374	hby0	ca672	1966	1:20000
Corralitos loamy sand, 2 to 9 percent slopes	CuC	3295	457377	hby3	ca672	1966	1:20000
Corralitos loamy sand, 9 to 15 percent slopes	CuD	1537	457378	hby4	ca672	1966	1:20000
Corralitos sand, 0 to 2 percent slopes	CtA	1141	457373	hbxz	ca672	1966	1:20000
Corralitos sand, 2 to 15 percent slopes, eroded	CtD2	528	457375	hby1	ca672	1966	1:20000
Corralitos loamy sand, 2 to 9 percent slopes	CoC	1245	457685	hc81	ca674	1968	1:24000
Corralitos loamy sand, 0 to 2 percent slopes	CoA	734	457684	hc80	ca674	1968	1:24000
Corralitos loamy sand	146	2770	458047	hcmq	ca678	1974	1:24000
Corralitos loamy sand, moderately fine substratum	147	480	458048	hcmr	ca678	1974	1:24000
Corralitos loamy sand	146	12	734860	snp5	ca679	1967	1:15840
Corralitos loamy sand, moderately fine substratum	147	1	818233	wgfm	ca679	1967	1:15840

Map of Series Extent

Approximate geographic distribution of the CORRALITOS soil series. To learn more about how this distribution was mapped, or to compare this soil series extent to others, use the Series Extent Explorer (SEE) application. Source: generalization of SSURGO geometry (updated 2024-10-30).